Vocabulary Earthquake- the shaking and trembling that results from the movement of rock beneath Earth's surface. Stress- a force that acts on rock to change its shape or volume. Shearing- stress that pushes a mass of rock in two opposite directions. Tension- a force that stretches rock to make it thinner. Compression- a force that squeezes rocks until it folds or breaks. Deformation- any change in the volume or shape of Earth's crust. Fault- a break in Earth's crust where slabs or crust slip past each other. Strike-slip Faults- a fault where rocks slip past each other sideways with little up-or-down motion. Normal Faults- a fault that has a hanging wall and footwall that slides downwards. Reverse faults- the exact opposite of a normal fault, which has a footwall and a hanging wall except sliding upwards. Friction- the force that opposes the motion of one surface as it moves across another surface. Fault-block Mountain- normal faults uplifting a block of rock. folds- bends in rock that form when compression shortens and thickens part of Earth's crust. Anticline- the fold in rock that bends upward into an arch. Syncline- a fold in rock that bends downward in the middle to form a bowl. Plateau- a large area of flat land elevated high above sea level.
Outline
Stress in the Crust
Stress
the force that changes the shape and volume of rock
adds energy to rock
Types of Stress
shearing
slip and breaks rock
***
* tension
pulls on crust
stretches rock, so it becomes thinner in the middle
compression
squeezes rock till folds or breaks
like a giant trash compactor
deformation
changes in the earth's crust
Kinds of Faults
faults
a break in earth's crust
faults occur near boundaries
Strike-Slip Fault
shearing
causes strike-slip fault
boundaries form
called transform boundary
Normal Faults
tension
causes normal faults
rock slips
fault that lies above is hanging wall
fault that lies below is footwall
Reverse Faults
compression
causes reverse faults
reverse faults produce part of Appalachian Mountain
Friction Along Faults
Friction
a force that opposes the motion of one surface as it moves across another surface
Faults sometimes jam together because of friction
they will jerk free, which produces small earthquakes
stress is strong enough to overcome friction force
Mountain Building
forces of plates can build up earth's surface
Mountains formed by Faulting
Fault block mountain
forms when faults uplift a block of rock
Sierra Nevada of California is a fault-block mountain
Great Basin also has many ranges of fault block mountain
two plates move away from each other
creates many normal faults
Mountains formed by Folding
Folds
plate movement causes crust to fold
bends in rock that form compression
California's northern Coast Range are partly the result of folding
Anticlines and Synclines
A fold in rock that bends upward into an arch is Anticline
anticline is the Black Hills
Black Hill formed about 65 million years ago
A fold in rock that bends downwards into an arch is Syncline
syncline can be as large as Illinois
The Illinois Basin is a syncline that stretches very far
Plateaus
plateaus
the force that raises mountains
a large area of flat land above sea level
a lot of plateau lies more than 1500 meters above sea level
Table of Contents
Earth's Crust in Motion
Vocabulary
Earthquake- the shaking and trembling that results from the movement of rock beneath Earth's surface.
Stress- a force that acts on rock to change its shape or volume.
Shearing- stress that pushes a mass of rock in two opposite directions.
Tension- a force that stretches rock to make it thinner.
Compression- a force that squeezes rocks until it folds or breaks.
Deformation- any change in the volume or shape of Earth's crust.
Fault- a break in Earth's crust where slabs or crust slip past each other.
Strike-slip Faults- a fault where rocks slip past each other sideways with little up-or-down motion.
Normal Faults- a fault that has a hanging wall and footwall that slides downwards.
Reverse faults- the exact opposite of a normal fault, which has a footwall and a hanging wall except sliding upwards.
Friction- the force that opposes the motion of one surface as it moves across another surface.
Fault-block Mountain- normal faults uplifting a block of rock.
folds- bends in rock that form when compression shortens and thickens part of Earth's crust.
Anticline- the fold in rock that bends upward into an arch.
Syncline- a fold in rock that bends downward in the middle to form a bowl.
Plateau- a large area of flat land elevated high above sea level.
Outline
Stress in the Crust
Types of Stress
- shearing
- slip and breaks rock
**** tension
Kinds of Faults
Strike-Slip Fault
Normal Faults
Reverse Faults
Friction Along Faults
Mountain Building
Mountains formed by Faulting
Mountains formed by Folding
Anticlines and Synclines
Plateaus
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